人类对全球河流悬浮沉积物的快速变化
Evan N Dethier1,2, Carl E Renshaw1, Francis J Magilligan3
1Department of Earth Sciences, Dartmouth College, Hanover, NH 03755, USA.
概括
由于人类活动, 全球河流沉积物量正在发生剧烈变化. 北方的水捕获沉积物,而南方的土地使用增加了侵蚀,将沉积物来源转移到南美洲.
科学领域:
- 环境科学
- 水文学
- 遥感技术
背景情况:
- 河流对生态功能,人类健康和基础设施至关重要.
- 有限的河流采样限制了对全球河流系统变化的理解.
- 在过去的50年里, 人类活动对全球的河流系统产生了重大影响.
研究的目的:
- 评估河流悬浮沉积物度和流量的全球变化.
- 将观察到的变化归因于特定的人类活动.
- 了解全球北方和南方之间的沉积物动态差异.
主要方法:
- 使用基于卫星的悬浮沉积物度和流量估计.
- 分析了全球414条主要河流的数据.
- 现在的沉积物动态与大前的条件和1980年代的数据进行了比较.
主要成果:
- 全球沉积物流量已经下降到大前的49%,主要是由于全球北部的水捕获沉积物.
- 全球南方的土地利用变化增加了侵蚀,自20世纪80年代以来,河流悬浮沉积物度平均上升了41%.
- 沉积物动力学中的一个显著的南北分歧正在重新配置全球沉积物流向海洋的模式,南美成为主要来源.
结论:
- 人类活动,特别是水建设和土地利用变化,是全球观测到的河流沉积物变化的主要驱动因素.
- 这项研究强调了全球河流沉积物来源的重大转变, 从亚洲迁移到南美.
- 了解这些动态对于管理河流生态系统和沿海环境至关重要.
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